Showing 241 - 260 results of 3,867 for search '"glacier"', query time: 0.18s Refine Results
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    Hydrodynamics and hydrogeochemistry of Werenskiold Glacier forefield, SW Spitsbergen by Magdalena Modelska, Sebastian Buczyński

    Published 2023-03-01
    “…The results indicate that the main source of water in the glacial river were the subglacial outflows in the central part of the glacier. They generated 77% of the total amount of water in the glacier forefield. …”
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    New glacier thickness and bed topography maps for Svalbard by W. van Pelt, T. Frank

    Published 2025-01-01
    “…<p>Knowledge of the thickness, volume, and subglacial topography of glaciers is crucial for a range of glaciological, hydrological, and societal issues, including studies on climate-warming-induced glacier retreat and associated sea level rise. …”
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    Applying a Mesoscale Atmospheric Model to Svalbard Glaciers by Björn Claremar, Friedrich Obleitner, Carleen Reijmer, Veijo Pohjola, Anna Waxegård, Florian Karner, Anna Rutgersson

    Published 2012-01-01
    “…The mesoscale atmospheric model WRF is used over three Svalbard glaciers. The simulations are done with a setup of the model corresponding to the state-of-the-art model for polar conditions, Polar WRF, and it was validated using surface observations. …”
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    Distributed surface mass balance of an avalanche-fed glacier by M. Kneib, M. Kneib, A. Dehecq, A. Gilbert, A. Basset, E. S. Miles, E. S. Miles, G. Jouvet, B. Jourdain, E. Ducasse, L. Beraud, A. Rabatel, J. Mouginot, G. Carcanade, O. Laarman, F. Brun, D. Six

    Published 2024-12-01
    “…<p>Local snow redistribution processes such as avalanches can considerably impact the spatial variability of accumulation on glaciers. However, this spatial variability is difficult to quantify with traditional surface mass balance measurements or geodetic observations. …”
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    Self-sufficient seismic boxes for monitoring glacier seismology by Ana Nap, Fabian Walter, Martin Lüthi, Adrien Wehrlé

    Published 2023-01-01
    “… Glacier seismology is a valuable tool for investigating ice flow dynamics, but sufficient data acquisition in remote and exposed glaciated terrain remains challenging. …”
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